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The tidal bore of the Garonne River, France

机译:法国加龙河的潮汐口

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摘要

A tidal bore is a series of waves propagating upstream as the tidal flow turns to rising. It forms during spring tide conditions when the tidal range exceeds 4 m to 6 m and the flood tide is confined to a narrow fun-neled estuary. In France alone, several tidal bores are observed (Figure 1). One most famous tidal bore on Earth was the mascaret of the Seine River (Malandain 1988). The Seine River tidal bore had had a sinister reputation: Its height could reach up to 7.3 m and the bore front travelled at a celerity of about up to 10 m/s (Bazin 1865, Tricker 1965). In the Baie du Mont Saint Michel, several tidal bore processes are experienced in creeks and rivers (Tessier and Terwindt 1994, Chanson 2004, 2008).
机译:潮流洞是随着潮流转向上升而在上游传播的一系列波。当潮汐范围超过4 m至6 m且洪水潮被限制在一个狭窄的漏斗河口时,它在春季潮汐条件下形成。仅在法国,就观察到了几个潮汐孔(图1)。地球上最著名的潮汐口是塞纳河的睫毛膏(Malandain 1988)。塞纳河(Seine River)潮汐口岸曾有过险恶的声誉:它的高度可达7.3 m,而井口的前行速度高达10 m / s(Bazin 1865,Tricker 1965)。在圣米歇尔山湾,在小溪和河流中经历了几次潮汐过程(Tessier和Terwindt,1994; Chanson,2004,2008)。

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  • 来源
    《Shore and beach》 |2011年第4期|p.51-54|共4页
  • 作者

    Hubert Chanson;

  • 作者单位

    Professor, School of Civil Engineering, The University of Queensland, Brisbane QLD 4072, Australia;

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  • 正文语种 eng
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